Zambezi River Zambezi River T he Zambezi is Africa’s fourth largest River system, after the Nile, Zaire and Niger Rivers. It runs through six countries on it’s journey from central Africa to the Indian Ocean. Its unique value is that it is less developed than others in terms of human settlement and many areas along it’s banks enjoy protected status. It’s power has carved the spectacular Victoria Falls and the zigzagging Batoka Gorge. The Zambezi has been harnessed at various points along the way including the massive Kariba Dam between Zambia and Zimbabwe and Cabora Bassa Dam in Mozambique. Plans for another dam at the Batoka gorge have fortunately been shelved. The River’s beauty has attracted tourists from all over the world providing opportunities for a myriad of water sports and game viewing. Running for a length of 2700kms, it begins it’s journey as an insignificant little spring in the corner of north-west Zambia in the Mwinilunga District. It bubbles up between the roots of a tree, very close to the border where Zambia, Angola and Zaire meet.

It enters Angola for about 230kms, where it accumulates the bulk of its headwater drainage, and re-enters Zambia again at Cholwezi rapids flowing due south but substantially enlarged by the entry of various tributaries. This upper part of the river is thinly populated by pastoralists, farmers and fishermen and although wildlife is sparse it is remarkably free of pollution. This is also the scene of the remarkable Ku-omboka Ceremony where thousands of inhabitants move annually to higher ground as the Zambezi floods into the low lying plains. It passes through the flat sandy country of the Western Province, then traverses the broad, annually flooding Barotse Plains, where much of the water is lost to evaporation, then over more rocky country where it’s tranquil course is interrupted by the Ngonye falls and rapids. As it turns to an easterly direction it forms the border between Zambia and Namibia and eventually joins up with the Chobe River in the Caprivi Swamps, briefly forming a border with Botswana.

For the next 500kms it serves as the border between Zambia and Zimbabwe thundering over the Victoria Falls and through the narrow, steadily deepening Batoka Gorge, providing a fantastic playground for white water rafting, kayaking, river boarding and jet boating. From here the steep sides of the gorge eventually flatten out at the broad Gwembe Valley. Then it flows into the Kariba dam for 281kms – it’s width at one point being 40kms. From the dam wall the river travels due north, heading east again at Chirundu. Here it is flanked by the Lower Zambezi National Park on the Zambian side and Mana Pools National Park on the Zimbabwean side. This middle zone supports one of Africa’s most important wilderness areas. After the Luangwa confluence, it’s a much larger Zambezi that flows into Mozambique and out towards the Indian Ocean, having provided power, food, pleasure and transport for many and a home for untold numbers of wildlife along it’s journey.

Fishing Trips on the Zambezi River To The Victoria Falls : The Zambezi River To The Victoria Falls A Natural Wonder The Zambezi River It is thought Zambezi means ‘Great River’ in the language of the Tonga people who inhabit its middle reaches. However the Lozi refer to the river as 'yambezhi' (pronounced 'le-am-by'), meaning 'heart of all', but it is possible the name has common ancestory in both languages. For many years the river was spelt 'Zambesi', with the now popular spelling of 'Zambezi' becoming only widely used in the latter half of the last century. The Zambezi River is the forth longest river in Africa (after the Nile, Congo, and Niger) and the largest to discharge into the Indian Ocean from the African continent, flowing for about 2,574 kilometres from its source on the Central African Plateau to sea. Rising in Zambia at a height of 1,524 metres above sea level, the Zambezi flows through, or borders, six countries (Zambia, Angola, Namibia, Botswana, Zimbabwe and Mozambique) before discharging into the Indian Ocean.

The Zambezi River basin catchment area extends over the territory of eight countries - Zambia, Angola, Namibia, Botswana, Zimbabwe, Malawi, Tanzania and Mozambique - a catchment area of 1,320,000 km2 with a cumulative mean annual flow of approximately 97 km3 - making it the largest river in southern Africa. By comparison the Zambezi roughly equates to the Nile, but is significantly less than the annual flow of the Congo, which in turn is significantly less than that of the Amazon. The river is generally separated into three sub-sections, representing its different physical and biological characteristics. The coastal section, or Lower Zambezi , stretches 360 miles up as far as the Cahora Bassa gorge, now flooded by the Cahora Bassa Dam. The Middle Zambezi is 600 miles long, in low-lying country, and is divided from the Upper Zambezi regions of the river by the Victoria Falls, 1,000 miles from the coast.

Map of the Zambezi River basin (highlighted) within southern African context The wider Zambezi River Basin is home to some forty million people who speak Bantu-lineage local languages with English and Portuguese being the main official languages. The Basin is well endowed with mineral, water and energy resources, natural tourist attractions like the Victoria Falls, as well as a healthy wildlife population. Major Tributaries of the Zambezi River The Zambezi has a number of important tributaries, which constitute major rivers in their own right, including the Shire River, flowing from the territories of Tanzania, Malawi and Mozambique, the Luangwa, Kafu and Kabompo rivers, lying wholly within Zambia, the Luena, from the territory of Angola and Zambia, and the Cuando (or Kwando), also known as the Chobe, draining from Angola, Namibia and Botswana. The most westerly of these is the Cuando (or Kwando), draining an area from Angola, Namibia and Botswana. Following a south-easterly course as far as the Botswana–Namibia border, it veers sharply northeastwards to link with the Zambezi via the Linyanti-Chobe floodplain.

The mid-section of the Cuando is a floodplain, comparable with the Barotse floodplain, and linked to the latter by a broad belt of alluvium termed the Mulonga-Matebele Plain, which is subject to flooding in the wet season. The Kafue is a north bank tributary with headwaters on the Southern Equatorial Divide. It initially flows in a general southwesterly direction towards the Upper Zambezi, but the course veers sharply eastwards in the vicinity of a broad floodplain known as the Kafue Flats. This tributary links with the Mana Pools Basin of the Middle Zambezi below the deeply incised Kafue Gorge. The Luangwa River flows in a general south-westerly direction over most of its length – an unusual orientation for a major tributary of an east-draining river. The course veers sharply to the south-south-east a little above the confluence with the Zambezi in the upper reaches of the Chicoa Basin. The mid-Zambezi has a number of relatively minor south bank tributaries, which rise on the central Zimbabwe divide. Their upper reaches flow in a general north-westerly direction.

A major tributary of the Lower Zambezi is the Shire, which flows southwards from its headwaters in Lake Malawi, in Malawi. Hydrology of the Zambezi Catchment The hydrology of the Zambezi catchment is determined by the annual variation of summer rainfall, which is influenced by the movement of the Intertropical Convergence Zone. The further south the zone moves, the greater the delivery of rainfall across the catchment. In winter these boundaries move north, resulting in drier conditions across the Zambezi Basin. River hydrology is further influenced by man. Off-take for agricultural, industrial and domestic use only amounts to about 3 percent of the total flow of the river. Use by hydro-electric facilities, due to the evaporation lost from the large surface area of reservoirs such as Kariba and Cabora Bass Dams, amounts to just over 5 percent of flow. Usage by these sectors is however likely offset by the increased runoff caused by deforestation, drainage of wetlands and other changes in landuse.

(Studies on Lake Malawi (Price et al 1998) indicates that increased runoff caused by the clearing of natural forests in the Shire catchment has meant the level of Lake Malawi in the early 1990s was 1m higher than it would have been otherwise). The annual variation in rainfall between dry winters and wet summers produce high flows in February-April and then progressively lower flows up to a November minimum. The annual flooding is however buffered by the natural flood regulatory capacity of the floodplains developed on the major headwater tributaries. The most important of these are the Barotse and Chobe floodplains in the upper Zambezi, the Kafue Flats on the Kafue River and Elephant March on the Shire River [major tributaries of the Zambezi]. Flow has been further affected by the construction of major dams in the Zambezi (Kariba and Cahora Bassa) and on the Kafue (Itezhi tezhi and Kafue Gorge).

(Gupta, 2007) The extensive wetland areas along the Zambezi, in particular the Upper Zambezi catchment are important biodiversity hotspots as well as playing a crucial role in regulating floodwaters. 'The densely vegetated floodplains such as the Barotse and Chobe (Upper Zambezi) and the Kafue Flats, with their shallow gradients, form natural sediment traps that greatly reduce the material supplied to the lower reaches of the river system. These floodplains as a consequence form major wetlands that provide important wildlife refuges, particularly for fish, avifauna and water-dependent mammals, including hippopotamus and the lechwe and sitatunga antelopes. Fish migrate into the inundated grasslands of the floodplains during the floods, spawn, and their fry utilize the rich plankton and benthic communities which develop after nutrient release from decomposing organisms drowned by the floodwaters. Readily accessible stretches of the Zambezi and major tributaries, such as the Barotse floodplain, provide a reliable perennial water source, and are thus an important focus for human settlement and agricultural activity (Davies, 1986).

(Gupta, 2007) Zambezi River Profile Damming the Zambezi As well as Kariba and Cahora Bassa Dams on the Zambezi itself, two other major dams, the Itezhi tezhi and Kafue Gorge Dams have been built on the Kafue, a major tributary of the river. There have been marked changes to the ecology and utilization of the Zambezi River system as a result of the construction of several major dams, such as Kariba Dam and Cabora Bassa on the middle Zambezi, and the Itezhi tezhi and Kafue Gorge Dams on the Kafue. These impoundments had a major impact on the economy of the region. Thus, they represent an important source of hydroelectricity for the whole subcontinent, where there is a rapidly rising demand for power. The introduction of the Lake Tanganyika sardine Limnothrissa miodon (colloquially known as ‘kapenta’) into Lake Kariba in 1967 has formed the basis of an important fishing industry.

Against all expectations, this fish survived discharge via the Kariba turbines and sluice gates, as well as a journey of several hundred kilometres to colonise Cahora Bassa, where it now also forms the basis of an important fishing industry (Davies, 1986; Jackson, 2000). The large dams have also become the focus of an important tourist industry. Nevertheless, these economic benefits have come at considerable human and ecological costs. The construction of Lake Kariba led to the displacement of about 50,000 members of the Tonga tribe which had inhabited the area since about 1100 AD, while about 25,000 people were relocated as a result of the construction of Cahora Bassa. These displacements have led to serious community disturbances, major psychological upsets and emotional problems in the attempt to adapt to new terrain and a new way of life, and bitterness and resentment that rankles to this day (Davies, 1986). The dams have also had severe ecological impacts on the major floodplains, as a result of the reduction of the supply of water and sediment.

The resultant contraction of these wetlands impacts particularly on fish, avifauna and water-dependent antelope species, and are only marginally offset by the added wetlands of the lake shallows (Davies, 1986). This is well illustrated by the collapse in numbers of the semi-aquatic Kafue lechwe (Kobus kafuensis), which is endemic to the Kafue flats, following construction of the Itezhi-tezhi Dam. Today, this species is confined to a fragment of the former range, with a decline from an estimated population of 350,000 at the turn of the twentieth century to less that 30,000 today (Cotterill, 2005). It has also been estimated that the closure of Cahora Bassa led to a 70% reduction of the supply of sediment to the lower reaches of the river, and that this could lead to severe erosion of the Zambezi Delta, threatening both agricultural activity and the important Marromeu wilderness area. During the annual floods prior to construction of the dams, the drowned grasslands of the delta were protected from overgrazing, and thus able to regenerate.

The virtual elimination of the natural flooding regime has disturbed this important ecological dynamic. It may also be responsible for the present marked die-off of the coastal mangroves, and the catastrophic decline of the coastal shrimp-fishing industry (Davies, 1986). The latter author notes that a major problem in quantifying the ecological effects of the construction of the major dams was the lack of baseline environmental data prior to their construction. (Gupta, 2007) In addition to these exitsting dams, it is also proposed to build hydro-electric dam facilities at the Batoka Gorge and Devil's Gorge, both above Kariba, and the Mupata Gorge, between Kariba and Cahora Bassa. These sites were first identified in 1973, and have been proposed repeatedly over the years. As of early 2013 Zimbabwe and Zambia were in advanced stages of planning for the construction of the Batoka Gorge Dam, which will flood the Zambezi at a maximum level to within 5 metres of the base outflow for the Victoria Falls Hydro-electric station. The dam is due for completion in 2019.

The other two damns are looking increasingly likely as the region is predicted to suffer a widening energy deficit. For latest on the proposed Batoka Gorge Dam development please visit Victoria Falls Bits and Blogs Batoka Dam News (external site, opens in a new window). A sixth dam, not shown in the above diagram, is in the advanced stages of planning in Mozambique. Located 60 kilometres downstream of Cahora Bassa Dam has been a hot topic in recent years, being listed as possibly the least environmentally friendly dam in Africa. Zambezi River Dams, planned and constructed [Source: Zambezi River Authority] Management of the Kariba and other hydro-electric facilities requires a network of of thirteen hydrological stations where water levels are monitored daily. Flow measurements are also carried out at eight stations. Major Towns along the Zambezi Along much of the river's length, the population is sparse, but important towns and cities along its course include Katima Mulilo (Namibia), Mongu, Lukulu, Sesheke and Livingstone (Zambia), Victoria Falls and Kariba (Zimbabwe) and Songo and Tete (Mozambique).

Tete continues to dominate the centre-west part of the region, and is the largest settlement along the length of the Zambezi. Crossing the Zambezi The Zambezi is a major geographic boundary and barrier to land based transport. Historically control of the river by the Lozi and TokaLeya boatmen was strategically important to protecting their kingdoms from Matabele (Ndebele) raids, and access to the Barotse heartlands were strictly controlled through strategic crossing points such as Kazungula. Over its entire course, the Zambezi is spanned by only a few bridges: in the upper Zambezi at Chinyingi by a simple suspension bridge and in the Caprivi the Katima Mulilo bridge; in the middle Zambezi the Victoria Falls bridge and two bridges at Chirundu; and in the lower Zambezi sections the Tete suspension bridge and Dona Anna bridge. There are two major ferry crossings, at Kazungula (between Zambia and Botswana) and Caia (in Mozambique). The Cazombo road bridge in Angola was bombed in the civil war and has not yet been reconstructed.

The Katima Mulilo Bridge carries the TransCaprivi Highway over the Zambezi River between Katima Mulilo, Namibia and Sesheke, Zambia. It is a road bridge, completed in 2004, 900 metres long and with 19 spans. The Victoria Falls Bridge was constructed in 1904/5 as a railway bridge and part of Cecil Rhodes's failed scheme for a trans-continental railway stretching the length of Africa. Its location, so close to the Victoria Falls, was not without controversy at the time. At the time of its construction it was claimed to be the highest bridge over water in the world. The bridge was originally designed only to carry railway traffic, supporting two sets of rails, but in 1929/30 the top deck was reconstructed, with only one set of rails, a road and pedestrian footways. Originally known as the Zambesi Bridge, with the construction of later bridges it became known as the Victoria Falls Bridge. The Otto Beit Bridge is a single-lane bridge built in 1938-9 by the Cleveland Bridge Company, the same builders as the Victoria Falls Bridge.

The Otto Beit Bridge was the first modern suspension bridge outside the United States built with parallel wire cables. It has a span of 382 m (main span 320 m). As it was built two decades before the Kariba Dam, the engineers had to consider the annual Zambezi flood, now tamed by the dam: hence the requirement for a single span (which the second bridge did not need). The second Chirundu Bridge is a two-lane, three-span continuous pre-stressed concrete box girder bridge, 400 meters long and 10.3 meters wide and was built in 2002. It is 90 metres upstream from the Otto Beit Bridge, using the same approaches and border control area. The one-kilometre-long Tete Suspension Bridge, finished in 1973 by the Portuguese and designed by Edgar Cardoso, is a major transportation facility in the region. The Dona Ana Bridge spans the lower Zambezi River in Mozambique, effectively linking the two halves of the country. It was originally constructed as a railway bridge in 1935 to link Malawi and the Moatize coal fields to the port Beira.

At that time, it was the longest railway bridge in Africa, with a length of about 3 km, and was known as the Zambezi Bridge (the old 'Zambesi Bridge' had by now become known as the Victoria Falls Bridge). In the 1980s, during the Mozambican Civil War, it was rendered unusable. In 1995, it was repaired with funds from USAID and converted to a single-lane bridge for vehicle traffic. The Dona Ana Bridge is the longest bridge to cross the Zambezi and currently the last before its mouth in the Indian Ocean. In 2007 construction started on the longest road bridge to span the Zambezi to replace the ferry at Caia, and which will become the last bridge before the mouth of the river. With a planned length of 2376 m and width of 16 m it will be exceeded only by the Dona Ana Bridge, which it is planned will be restored as a railway bridge. Above the Falls, the Kazungula Ferry is a pontoon ferry across the 400-metre-wide section of the Zambezi River between Botswana and Zambia.

It is one of the largest ferries in south-central Africa, having a capacity of 70 tonnes. The service is provided by two motorised pontoons and operates between border posts at Kazungula, Zambia and Kasane, Botswana. It links the Livingstone-Sesheke road (which connects to the Transcaprivi Highway at Katima Mulilo) to the main north-south highway of Botswana and also to the Kasane-Victoria Falls road through Zimbabwe. Plans for a bridge to replace the ferry crossing are in development, with construction planned to begin towards the end of 2012. Zambezi River | river, Africa | Britannica.com Zambezi River Alternative Titles: Zambesi River, Zanbere River Related Topics Kariba Zambezi River, also spelled Zambesi, river draining a large portion of south-central Africa. Together with its tributaries, it forms the fourth largest river basin of the continent. The river flows eastward for about 2,200 miles (3,540 kilometres) from its source on the Central African Plateau to empty into the Indian Ocean .

With its tributaries, it drains an area of more than 500,000 square miles (1,300,000 square kilometres). The Zambezi (meaning “Great River” in the language of the Tonga people) includes along its course the Victoria Falls , one of the world’s greatest natural wonders, and the Kariba and Cahora Bassa dams, two of Africa’s largest hydroelectric projects. The river either crosses or forms the boundaries of six countries—Angola, Zambia, Namibia , Botswana , Zimbabwe , and Mozambique —and the use of its waters has been the subject of a series of international agreements. The Zambezi River basin and its drainage network. Encyclopædia Britannica, Inc. Victoria Falls on the Zambezi River as seen from Zambia. G. Holton/Photo Researchers The Zambezi River at sunset.

Art Wolfe—Stone/Getty Images Physical features Physiography The Zambezi rises out of a marshy bog near Kalene Hill, Zambia , about 4,800 feet (1,460 metres) above sea level , and flows some 20 miles before entering Angola , through which it runs for more than 175 miles. In this first section of its course, the river is met by more than a dozen tributaries of varying sizes. Shortly after reentering Zambia, the river flows over the Chavuma Falls and enters a broad region of hummocky, sand-covered floodplains, the largest of which is the Barotse, or Zambezi, Plain. The region is inundated during the summer floods, when it receives fertile alluvial soils. The main tributaries intersecting the river along the plains are the Kabompo River from the east and the larger Lungué-Bungo (Lungwebungo) River from the west.

Similar Topics Kagera River The Zambezi then enters a stretch of rapids that extends from Ngonye (Sioma) Falls south to the Katima Mulilo Rapids, after which for about 80 miles it forms the border between Zambia to the north and the eastern Caprivi Strip—an extension of Namibia—to the south. In this stretch the river meanders through the broad grasslands of the Sesheke Plain until it is joined by the Cuando ( Kwando ) River. Near Kazungula, Zambia, the river, after flowing past Botswana territory to the south, turns almost due east and forms the frontier between Zambia and Zimbabwe. From the Cuando confluence to the Victoria Falls , the Zambezi varies considerably in width, from open reaches with sand islands to stretches of rapids through narrow channels separated by numerous rock islands. The Victoria Falls mark the end of the upper course of the Zambezi, as its waters tumble with a thunderous roar and an enormous cloud of spray. The area around the falls was once covered by a thick layer of lava, which as it cooled formed wide cracks, or joints, that became filled with softer sediments.

As the Zambezi cut its present valley it encountered one of these joints, eroded the sediment, and created a trench, eventually forcing a gap at the lower end of the trench that quickly widened into a gorge. The force of the water also created a second gap at the upper end of the trench that gradually diverted the river until the trench itself was left dry. As the river cut backward it repeated the process, scouring eight successive waterfalls in the past half million years. The Zambezi’s middle course extends about 600 miles from Victoria Falls to the eastern end of Lake Cahora Bassa in Mozambique. It continues to form the boundary between Zambia and Zimbabwe until it crosses the Mozambique border at Luangwa. Below the falls a gorge some 60 miles long has been formed by the trench-scouring process, through which the river descends in a series of rapids. Just upstream of Lake Kariba the river valley widens and is contained by escarpments nearly 2,000 feet high. The middle Zambezi is notable for the two man-made lakes, Kariba and Cahora Bassa (see below), that constitute much of this stretch of the river.

Between the two lakes the Zambezi trends northeast for nearly 40 miles before it turns east below the confluence with the Kafue River , the Zambezi’s largest tributary. In this section the river rushes through two rocky, narrow gorges, the first just below the Kariba Dam and the other above the confluence with the Luangwa River . Britannica Stories Obama Acts to Protect the Arctic At the dam at the eastern end of Lake Cahora Bassa, the Zambezi begins its lower course, during which it descends from the Central African Plateau to the coastal plain . At first the hilly country is replaced by flat areas at the head of the Tete Basin, and the river becomes more placid. About 40 miles downstream the river has cut the Lupata Gorge through a range of hills, where it emerges onto the Mozambique Plain and occupies a broad valley that spreads out in places to a width of three to five miles. Near Vila Fontes the river receives its last great tributary, the Shire River , which drains Lake Nyasa (Malaŵi) some 210 miles to the north. Africa at Random: Fact or Fiction?

At its mouth the Zambezi splits into a wide, flat, and marshy delta obstructed by sandbars. There are two main channels, each again divided into two. The wider, eastern channel splits into the Muselo River to the north and the main mouth of the Zambezi to the south. The western channel forms both the Inhamissengo River and the smaller Melambe River. North of the main delta the Chinde River separates from the Zambezi’s main stream to form a navigable channel leading to a shallow harbour. Hydrology The Zambezi, according to measurements taken at Maramba (formerly Livingstone), Zambia, experiences its maximum flow in March or April. In October or November the discharge diminishes to less than 10 percent of the maximum. The annual average flow reaches about 247,000 cubic feet (7,000 cubic metres) per second. Measurements taken at Kariba Dam reflect the same seasonal pattern; the highest flood recorded there was in March 1958, when the flow reached 565,000 cubic feet per second. Climate Facebook Twitter YouTube Instagram Pinterest The Zambezi River lies within the tropics.

The upper and middle course of the river is on an upland plateau, and temperatures, modified by altitude, are relatively mild, generally between 64° and 86° F (18° and 30° C). The winter months (May to July) are cool and dry, with temperatures averaging 68° F (20° C). Between August and October there is a considerable rise in average temperatures, particularly in the river valley itself; just before the rains begin in October temperatures there become excessively hot, often reaching 104° F (40° C). The rainy season lasts from November to April. Rain falls in short, intense thundershowers—the rate sometimes reaching 6 inches (150 millimetres) per hour—with skies clearing between downpours. In these months the upper Zambezi receives nearly all its total rainfall, and this accounts for the great variation in the flow of the river throughout the year. In all, the upper and middle Zambezi valley receives 22 to 30 inches of rain per year.

Studies have suggested that a microclimate in the area of Lake Kariba has created a rise in precipitation, possibly as a result of a lake breeze blocked by the escarpment that produces thunderstorms. In the lower course of the river in Mozambique the influence of the summer monsoon increases the levels of precipitation and humidity. Temperatures are also higher—determined more by the latitude and less by altitude—as the river descends from the plateau. Plant life The vegetation along the upper and middle course of the Zambezi is predominantly savanna , with deciduous trees, grass, and open woodland. Mopane woodland (Colophospermum mopane) is predominant on the alluvial flats of the low-lying river valleys and is highly susceptible to fire. Grass, when present, is typically short and sparse. Forestland with species of the genus Baikiaea, found extensively on sandy interfluves between drainage channels, is economically the most important vegetation type in Zambia, for it is the source of the valuable Rhodesian teak (Baikiaea plurijuga). Destruction of the Baikiaea forest results in a regression from forest to grassland , a slow process involving intermediate stages of scrub vegetation.

The river additionally has a distinct fringing vegetation, mainly riverine forest including ebony (Diospyros mespiliformis) and small shrubs and ferns (e.g., Haemanthus). In the lower course of the Zambezi, dense bush and evergreen forest, with palm trees and patches of mangrove swamp, is the typical vegetation. Animal life About the Zambezi River Photo Gallery About the Zambezi River The Zambezi is Africa’s fourth-largest river and is one of the finest and least spoilt rivers in the world. Its source rises from a tiny spring in North-western Zambia and flows for 2,700 kms into the Indian Ocean at its delta on the Mozambique coast. Its basin (if you include all the river’s tributaries) covers most of central and southern Africa; an area of some 1.3 million sq. kms. – larger than the Sahara Desert. Eight countries in the region are directly linked into this vast river system – Zambia, Angola, Namibia, Botswana, Zimbabwe, Malawi, Tanzania and Mozambique. Map showing the area encompassed by the Zambezi River and its catchment area.

The Zambezi is one of Africa’s last remaining wild rivers. Its spectacularly beautiful attractions include one of the Seven Wonders of the World; Victoria Falls and its four gorges: the Batoka, Kariba, Mupata and Lupata as well as two man-made lakes: Kariba and Cabora Bassa. The river basin also incorporates several of Africa’s finest National Parks and safari areas and its magnificent delta has, for centuries been a focal point in the history and culture of the region. On June 3rd 2010, the International Coordinating Council of UNESCO’s Man and the Biosphere (MAB) Programme declared Zimbabwe’s Middle Zambezi Valley a Biosphere Reserve. This designation is a first for Zimbabwe and will allow us to test different approaches to integrated management of terrestrial, freshwater, coastal and marine resources and biodiversity. Zimbabwe’s new Middle Zambezi Biosphere Reserve stretches over approximately 40,000 sq. km in the Zambezi valley.

It includes riverine and terrestrial ecosystems unique to Southern Africa, one of its largest man-made reservoirs, Lake Kariba, and two core National Park areas: the Matusadona National Park on the Lake Kariba’s southern shores, and the UNESCO World Heritage Site of Mana Pools National Park, Sapi and Chewore safari areas , declared in 1984. Map showing the area encompassed by Zimbabwe’s Middle Zambezi Biosphere Reserve The Zambezi basin is rich in biological diversity. Its wetlands, aquatic systems, riverine woodlands, montane forests, dry forests and savannahs are all complex eco-systems which support abundant wildlife and a great diversity of trees and plants; some species native only to the Zambezi region. As a result, the Zambezi basin holds many wonderful wilderness landscapes and many natural resources that are of exceptional value.

However, the Zambezi River’s wild nature faces many threats: Poverty forces people into poaching of important Zambezi species like the Black Rhino, Elephant and Leopard, or unsustainable harvesting of forests and fish Developments such as high-impact agriculture, mining, energy generation, water extraction and ill-advised tourism developments are often prioritized over the preservation of wilderness for tourism, hunting or conservation Land planning in the eight Zambezi region countries lacks co-ordination, and is often haphazard. Local communities are seldom properly informed or consulted. What happens in the upper catchment area can have drastic environmental consequences on people and wildlife far downstream. Unlike most places in the world today, options for development in the Zambezi basin are still open. The Zambezi Society believes that this is a perfect opportunity for planners, decision-makers and conservationists to avoid the mistakes made elsewhere. THE ZAMBEZI SOCIETY’S MISSION IS TO PROMOTE THE CONSERVATION AND ENVIRONMENTALLY SOUND MANAGEMENT OF THE ZAMBEZI RIVER AND ITS CATCHMENT AREA FOR THE BENEFIT OF WILDERNESS, WILDLIFE AND PEOPLE.

Make a Donation to Support The Zambezi Society Visit the secure online payment gateway here: Rivers of Life: River Profiles - the Zambezi THE ZAMBEZI RIVER The Bundu people of Zambia believe the Zambezi River has a spirit called Nyami Nyami. This spirit brings them water to grow crops and fish to eat so they call the river "the river of life". The Zambezi originates in Northwestern Zambia, formerly Rhodesia, and flows through Angola, Botswana, Zimbabwe, and finally to Mozambique. Here it empties into the Indian Ocean 1600 miles from its headwaters. The climate along the river is considered tropical and the rainy season lasts from October through April. The river changes at different spots along it, going from a placid flow in sandy plains to annually flooded plains to a tumbling river of falls and rapids. Perhaps the most spectacular spot along the river is in Zimbabwe at Victoria Falls. These falls are two times the size of Niagara Falls at 355 feet high and 5500 feet wide! The Zambezi River is widely used by wildlife and humans alike.

Hippos, crocodiles, baboons, elephants, hyenas and lions are some examples of wildlife you might find along the Zambezi. Humans use the river for transportation, irrigation, tourism and hydropower. The people who live along the river differ from country to country. English is the official language of the area though the different tribes along the banks of the Zambezi speak more than 70 other languages. Currently the countries along the river are at odds as to how to manage the river. In the future these countries must agree to manage "the river of life" so that its people can survive and its spirit can thrive. Zambezi River Activities Things to do on the Zambezi River T his magnificent river flows through 6 different countries in its way to the Indian Ocean journey of around 2700 kilometres. The river starts about 1500 metres above sea level in the Mwinilunga District, very close to the border of Zambia. It then flows through Zambia, Angola, Namibia and Botswana before tracking back along the border of Zambia and Zimbabwe. It finally ends in the delta in Mozambique and courses into the Indian Ocean.

It is a river which is mostly unexplored and holds a spiritual and majestic value in the lives of the communities that live around it. The river is a true spectacle for the visitor and there is a lot do in and around this feature of Zambia. Adventure Activities Here are some ideas to get you started on your visit to the Zambezi River: The Kuomboka Ceremony is an annual event that should not be missed if you find yourself anywhere near the Zambezi in late March or April. An entire village on the Zambezi floodplains in Western Province migrates up river in a grand ceremony that is quite something to be a part of. Click here for more info (link to Section of Traditional Ceremonies) River Cruises on the Upper Zambezi Devils Pool – The experience of Livingstone Island with a picnic and then a swim in Devils Pool on the very edge of Victoria Falls will be something you will never forget. Please bear in mind that this is a seasonal activity as water levels need to be safe for visitors. Zambezi River rafting – perhaps one of the most popular activities on the river. Bear in mind that some of the rapids are challenging, but you will be accompanied by a guide.

Grab a group of friends or your family and spend a fun-filled day tackling the great Zambezi. Wave boarding and surfing – this one is for the serious enthusiast. River boarding is done on the same section of water as the river rafting. For the surfers out there, this is a great opportunity to surf a river! Jet Boating – experience the power of these extraordinary boats which are able to carry 11 passengers. An experienced driver will take you through the white water rapids and twist and turn in mere inches of water. Bungee jumping – if adventure icon Bear Grylls can take the plunge off the Victoria Falls bungee, then this is your chance to do the same. The 111 metre drop is sure to get your adrenalin kicking. If this doesn’t sound like something for you, try the Gorge Swing or Rap jump further down the Gorge.

Fishing – with tiger fish, a variety of bream, Kafue pike and Vundu catfish found in the upper Zambezi River, and Chessa, Nkupi, Bottlenose, Cornish Jack and a variety of Bream found in the Lower Zambezi, there is plenty of fishing to be done. Fishing trips spanning a number of days can also be organised by various operators. House Boating on Lake Kariba. The Zambezi runs into the wide Zambezi Valley and is held up by the massive hydro electric dam wall creating a vast lake offering watersports, fishing and house boating. The Lower Zambezi beyond the dam wall widens to a spectacular array of channels, frequented by elephants, buffalo, hippo, crocodiles and waterbirds. Here you can take a canoeing safari or river safaris with one of the lodges in the Lower Zambezi National Park. The Zambezi is a vast and captivating river. It draws many tourists each year to explore the exciting and interesting things to do. See the Victoria Falls page or the Livingstone page for other activities surrounding the Zambezi.

The Mighty Zambezi River and its wildlife - YouTube The Mighty Zambezi River and its wildlife Want to watch this again later? Sign in to add this video to a playlist. Need to report the video? Sign in to report inappropriate content. Rating is available when the video has been rented. This feature is not available right now. Please try again later. Published on Aug 11, 2012 The Zambezi (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, and the largest flowing into the Indian Ocean from Africa. The area of its basin is 1,390,000 square kilometres (540,000 sq mi),[1][2] slightly less than half that of the Nile. The 3,540-kilometre-long river (2,200 mi) has its source in Zambia and flows through eastern Angola, along the eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses that country to empty into the Indian Ocean. The Zambezi's most well-known feature is Victoria Falls. Category

Question: In which country does the Zambezi river empty into the Indian ocean?
Answer: Mozambique